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- W2030996811 abstract "Banded iron-formations (BIFs) occur in the Precambrian geologic record over a wide time span. Beginning at 3.8 Ga (Isua, West Greenland), they are part of Archean cratons and range in age from about 3.5 until 2.5 Ga. Their overall volume reaches a maximum at about 2.5 Ga (iron-formations in the Hamersley Basin of Western Australia) and they disappear from the geologic record at about 1.8 Ga, only to reappear between 0.8 and 0.6 Ga." @default.
- W2030996811 created "2016-06-24" @default.
- W2030996811 creator A5069889734 @default.
- W2030996811 date "2005-10-01" @default.
- W2030996811 modified "2023-10-14" @default.
- W2030996811 title "Some Precambrian banded iron-formations (BIFs) from around the world: Their age, geologic setting, mineralogy, metamorphism, geochemistry, and origins" @default.
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- W2030996811 doi "https://doi.org/10.2138/am.2005.1871" @default.
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